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雄安新区D01井岩溶热储下伏太古界中热流测定研究

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姚亚辉, 贾小丰, 李胜涛, 张建伟, 宋健, 杨涛, 岳冬冬. 2022. 雄安新区D01井岩溶热储下伏太古界中热流测定研究[J]. 中国地质, 49(6): 1723-1731. doi: 10.12029/gc20220602
引用本文: 姚亚辉, 贾小丰, 李胜涛, 张建伟, 宋健, 杨涛, 岳冬冬. 2022. 雄安新区D01井岩溶热储下伏太古界中热流测定研究[J]. 中国地质, 49(6): 1723-1731. doi: 10.12029/gc20220602
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YAO Yahui, JIA Xiaofeng, LI Shengtao, ZHANG Jianwei, SONG Jian, YANG Tao, YUE Dongdong. 2022. Heat flow determination of Archean strata under the karst thermal reservoir of D01 well in Xiong'an New Area[J]. Geology in China, 49(6): 1723-1731. doi: 10.12029/gc20220602
Citation: YAO Yahui, JIA Xiaofeng, LI Shengtao, ZHANG Jianwei, SONG Jian, YANG Tao, YUE Dongdong. 2022. Heat flow determination of Archean strata under the karst thermal reservoir of D01 well in Xiong'an New Area[J]. Geology in China, 49(6): 1723-1731. doi: 10.12029/gc20220602
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雄安新区D01井岩溶热储下伏太古界中热流测定研究

  • 1.

    中国地质调查局水文地质环境地质调查中心, 天津 300304

  • 2.

    天津市地热资源勘查开发工程研究中心, 天津 300304

  • 3.

    中国矿业大学资源与地球科学学院, 江苏 徐州 221116

  • 4.

    自然资源部地质环境监测工程技术创新中心, 天津 300304

  • 基金项目:
    国家重点研发计划(2020YEE0201300, 2018YFC0604305，2019YFB150410301)及中国地质调查项目(DD20189113，DD20190127，DD20221680)联合资助
详细信息
    作者简介: 姚亚辉, 男, 1990年生, 博士生, 工程师, 主要从事地热地质与水工环地质工作; E-mail: yaoyahui@mail.cgs.gov.cn
    通讯作者: 贾小丰, 男, 1982年生, 硕士, 高级工程师, 主要从事地热(干热岩)资源调查评价、二氧化碳地质储存潜力评价等方面的研究; E-mail: jiaxiaofeng@mail.cgs.gov.cn

  • 中图分类号: P314

Heat flow determination of Archean strata under the karst thermal reservoir of D01 well in Xiong'an New Area

  • 1.

    Center For Hydrogeology and Environmental Geology, China Geological Survey, Tianjin 300304, China

  • 2.

    Tianjin Engineering Center of Geothermal Resources Exploration and Development, Tianjin 300304, China

  • 3.

    School of Resource and Earth Science, China University of Mining and Technology, Xuzhou 221116, Jiangsu, China

  • 4.

    Technology Innovation Center for Geological Environment Monitoring Engineering, MNR, Tianjin 300304, China

  • Fund Project: Supported by the National Key Research and Development Program (No.2020YEE0201300, No.2018YFC0604305, No.2019YFB150410301) and the project of China Geological Survey (No.DD20189113, No.DD20190127, No.DD20221680)
More Information
    Author Bio: YAO Yahui, male, born in 1990, doctor candidate, engineer, mainly engaged in the research of geothermal geology, hydrogeology, engineering geology and environmental geology work; E-mail: yaoyahui@mail.cgs.gov.cn .
    Corresponding author: JIA Xiaofeng, male, born in 1982, master, senior engineer, mainly engaged in the geothermal and hot dry rock resource survey and the potential evaluation of CO2 geological storage; E-mail: jiaxiaofeng@mail.cgs.gov.cn

    摘要
  • 研究目的

    目前雄安新区范围内的热流数据多测自于新近系沉积盖层及白云岩地层，对岩溶热储下伏太古界的热流测定研究还鲜见报道，主要受限于以往的地热勘查开发层位主要在1800m以浅的蓟县系岩溶热储，揭露岩溶热储下伏太古界的钻孔稀少。2018年以来，在雄安新区牛驼镇地热田实施了D01深部地热参数井，揭穿了高于庄组岩溶热储，并揭露太古界厚度达1723.67m，给该地区岩溶热储下伏太古界的热流测定研究提供了条件。

     研究方法

    本文基于近稳态钻孔测温及岩心热导率测试，对D01井太古界进行了热流测定及分析。

     研究结果

    结果表明：D01井太古界呈显著的传导型地温特征，地温梯度为18.3℃/km，相比于新近系地温梯度48.6℃/km偏低。测得25块D01井太古界片麻岩岩心样品的热导率平均值为(2.41±0.40)W/(K·m)。根据钻孔测温数据及热导率测试，计算出D01井太古界2300~2700m深度的热流值为(44.1±7.0)mW/m2。同时，估算了D01井新近系400~800m深度段的热流值为84.6mW/m2，较太古界高出40.5mW/m2。

     结论

    分析认为D01井新近系较太古界高出热流主要为高孔渗岩溶白云岩层中地下水侧向热对流作用以及牛东断裂地下水垂向热对流作用共同所致。研究结果对前人提出的地下水运移聚热模式及导热断裂聚热模式提供了数据支撑，对雄安新区深部地热资源成因机制和太古界地温场研究具有重要意义。
    The paper is the result

    of geothermal geology survey engineering.

     Objective

    The heat flow values in Xiong'an New Area are mostly measured from the Neogene sedimentary cap and dolomite strata. The previous geothermal exploration and utilization horizons are mainly karst thermal reservoirs shallower than 1800m in the Jixian System and the boreholes exposing the Archean are scarce in Xiong'an New Area. Heat flow determinations and analyses from Archean under the karst thermal reservoir are rarely reported by previous researchers. Since 2018, D 01 deep geothermal parameter well with a depth of 3403.67m has been implemented in Niutuozhen geothermal field in Xiong'an New Area. The karst thermal reservoir of the whole Gaoyuzhaung Formation was exposed and the Archean of 1723.67m was drilled by D01 well. The D01 well provides the conditions for the heat flow study from Archean under the karst thermal reservoir in this area.

     Methods

    Based on borehole temperature measurement and thermal conductivity tests, the study on the heat flow from the Archean of D01 well was carried out.

     Results

    The results showed that the Archean of D01 well has significant geothermal characteristics of conduction type, and the geothermal gradient is 18.3℃/km, which is lower than the Neogene geothermal gradient of 48.6℃/km. The thermal conductivity values of 25 Archean gneiss core samples of D01 well were measured with an average value of (2.41±0.40) W/(K·m). Based on the temperature measurement curve and thermal conductivity data of 2300-2700m section of D01 well, the Archean heat flow of D01 well was calculated to be (44.1±7.0) mW/m2. The heat flow of the Neogene sedimentary cap of D01 well was estimated to be 84.6 mW/m2.

     Conclusions

    The higher part 40.5 mW/m2 than Archean of D01 well was considered to be mainly contributed by the lateral convection heat transfer of groundwater in high pore-permeable karst dolomite and the vertical convection heat transfer of groundwater in the Niudong fault. The research results can provide the basic data for the previous heat accumulation mechanism of the groundwater transport and the heat conduction fault. And the results are of great significance to the genetic mechanism of deep geothermal resources and the geothermal field of Archean in Xiong'an New Area.
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  • 图 1  渤海湾盆地构造单元图(a)和牛驼镇凸起基岩地质简图(b)(改自马敬业等，1990)

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  D01井钻遇地层柱状图

    Figure 2. 

    下载: 全尺寸图片 幻灯片

    图 3  D01井近稳态测温曲线

    Figure 3. 

    下载: 全尺寸图片 幻灯片

    图 4  新近系(a)和太古界(b)热流计算段测温数据线性拟合

    Figure 4. 

    下载: 全尺寸图片 幻灯片

    图 5  DR井静井261 d后测温曲线(Jiang et al., 2016)

    Figure 5. 

    下载: 全尺寸图片 幻灯片

    图 6  牛驼镇凸起地热地质概念模式图(地层剖面改自王贵玲等，2018)

    Figure 6. 

    下载: 全尺寸图片 幻灯片

    表 1  D01井太古界片麻岩岩心热导率测试统计

    Table 1.  Thermal conductivity of Archean gneiss core samples in D01 well

    下载: 导出CSV

    表 2  D01井和DR井分段热流对比

    Table 2.  Comparison of heat flow between D01 well and DR well

    下载: 导出CSV
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收稿日期:  2020-10-09
修回日期:  2020-11-21
刊出日期:  2022-12-25

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